The transition between the middle atmosphere and the thermosphere is known as the MLT
region (for mesosphere and lower thermosphere). This area has some characteristics that …

The background ionospheric conditions shaped by sunset electrodynamic processes are
responsible for the development of equatorial plasma bubble (EPB)/equatorial spread F …

Large ionospheric variability is found at low to middle latitudes when a quasi‐stationary
planetary wave is specified in the winter stratosphere in the National Center for Atmospheric …

Equatorial spread F (ESF) was discovered almost a century ago using the first radio wave
instrument designed to study the upper atmosphere: the ionosonde. The name came from …

In this study, we quantify the contribution of individual large‐scale waves to ionospheric
electrodynamics and examine the dependence of the ionospheric perturbations on solar …

Abstract Coincident Ionospheric Connections Explorer (ICON) measurements of neutral
winds, plasma drifts and total ion densities (:= Ne, electron density) are analyzed during …

Abstract The Thermosphere‐Ionosphere‐Mesosphere Electrodynamics General Circulation
Model (TIME‐GCM) is used to theoretically study the 6 day wave effects on the ionosphere …

Using the thermosphere‐ionosphere‐mesosphere electrodynamics general circulation
model simulations, we investigate the short‐term ionospheric variability due to the child …

Equatorial planetary scale wave modes such as Kelvin waves or Rossby-gravity waves are
excited by convective processes in the troposphere. In this paper an analysis for these and …

We report for the first time the day‐to‐day variation of the longitudinal structure in height of
the F2 layer (hmF2) in the equatorial ionosphere using multi‐satellite observations of …